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New fusulinid evidence for the Permian age of the Palaeozoic rocks of Hydra, Greece

Published online by Cambridge University Press:  01 May 2009

D. A. V. Stow
D. A. V. Stow
Affiliation:
Sidney Sussex CollegeCambridge
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Summary

The Palaeozoic rocks of Hydra consist of a sequence of limestones and dolomites with some interbeds of shales and sandstones. Fusulinid foraminifera indicate the sequence is entirely Permian in age and not Carboniferous and Permian as previously thought.

Type
Articles
Information
Geological Magazine , Volume 112 , Issue 1 , January 1975 , pp. 71 - 76
Copyright
Copyright © Cambridge University Press 1975

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References

Grant, R. E. 1972. The lophophore and feeding mechanism of the Productina (Brachiopoda). J. Paleont. 46, 213–49.Google Scholar
Ozawa, Y. & Tobler, A. 1929. Permian Fusulinidae found in Greece. Eclog. geol. Helv. 22, 45–9.Google Scholar
Renz, C. 1955. Die vorneogene Stratigraphie der normalsedimentären Formationen Griechenlands. 637 pp., Inst. geol. subsurf. Res., Athens.Google Scholar
Römermann, H. 1968. Geologie von Hydra. Geologica et Palaeontologica 2, 163–71.Google Scholar